1. Role of dynamic topography in sustaining the Nile River over 30 million years
- Author
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Thorsten W. Becker, Petar Glisovic, Zohar Gvirtzman, Alessandro M. Forte, Eduardo Garzanti, Andrea Sembroni, Claudio Faccenna, Faccenna, C., Glisovic, P., Forte, A., Becker, T. W., Garzanti, E., Sembroni, A., Gvirtzman, Z., Faccenna, C, Glisovic, P, Forte, A, Becker, T, Garzanti, E, Sembroni, A, and Gvirtzman, Z
- Subjects
010504 meteorology & atmospheric sciences ,Geodinamica, Evoluzione del Drenaggio, Nilo ,Geological evidence ,010502 geochemistry & geophysics ,01 natural sciences ,Mantle (geology) ,Paleontology ,Ocean surface topography ,Topographic gradient ,River nile ,Mantle convection ,Drainage system (geomorphology) ,General Earth and Planetary Sciences ,Drainage ,Geology ,0105 earth and related environmental sciences - Abstract
The Nile is the longest river on Earth and has persisted for millions of years. It has been suggested that the Nile in its present path is ~6 million years old, whereas others argue that it may have formed much earlier in geological history. Here we present geological evidence and geodynamic model results that suggest that the Nile drainage has been stable for ~30 million years. We suggest that the Nile’s longevity in essentially the same path is sustained by the persistence of a stable topographic gradient, which in turn is controlled by deeper mantle processes. We propose that a large mantle convection cell beneath the Nile region has controlled topography over the last 30 million years, inducing uplift in the Ethiopian–Yemen Dome and subsidence in the Levant Sea and northern Egypt. We conclude that the drainage system of large rivers and their evolution over time can be sustained by a dynamic topographic gradient. The path of the river Nile has been stable for as long as 30 million years, sustained by mantle convection, according to geophysical and geological evidence and geodynamic model simulations.
- Published
- 2019